Allanite-(Nd) is a rare member of the epidote group characterized by a dominance of neodymium in the rare-earth element site. It typically occurs as dark, opaque, prismatic crystals in granitic pegmatites and often exhibits metamictization due to internal radioactive decay. Collectors should look for distinct crystalline forms in pegmatitic environments associated with other rare-earth minerals.
Is this allanite-(nd)?
5-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch allanite-(nd) with a known reference. Allanite-(Nd) sits at Mohs 6, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: grayish brown.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: black, brownish black.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals, massive, granular.
Often confused with
Allanite-(Nd) vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Streak differs, so Allanite-(Nd) leaves grayish brown, Allanite-(Ce) leaves gray.


How to tell apart: Streak differs, so Allanite-(Nd) leaves grayish brown, Allanite leaves gray; luster reads vitreous on Allanite-(Nd) and submetallic on Allanite.
All properties
- Chemical formula
- CaNdAl₂Fe(Si₂O₇)(SiO₄)O(OH)
- Mohs hardness
- 6
- Density
- 3.98 g/cm³
- Colors
- Streak
- Grayish brown
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic crystals, massive, granular
- Cleavage
- Imperfect on {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- An accessory phase in the blocky zone of a NYF-type granitic pegmatite (Sweden)
Where rockhounds find allanite-(nd)
Classic worldwide localities
- Kingman pegmatite, Cerbat Range, ~1.5 km northwest of Kingman, Arizona, USA
- La Cabrera, Spain and Ryoke, Japan
Field-hunting tip
Where it forms: An accessory phase in the blocky zone of a NYF-type granitic pegmatite (Sweden). If you start seeing iimoriite-, keiviite-, allanite- in float, you are in the right ground. Typical habit: prismatic crystals, massive, granular. Train your eye for that shape before scanning the outcrop.
